Paxite is a rare copper arsenide mineral typically occurring as massive or granular aggregates in hydrothermal veins. It is most commonly found alongside other copper-arsenic minerals such as koutekite and domeykite. Identification is difficult without laboratory analysis like X-ray diffraction or electron microprobe study due to its resemblance to other silver-white metallic minerals.
Is this paxite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch paxite with a known reference. Paxite sits at Mohs 3.5 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Paxite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Paxite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: silver-white, gray.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: massive, granular.
Often confused with
Paxite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside paxite
Minerals reported to co-occur with paxite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Cu₂As₃
- Mohs hardness
- 3.5
- Density
- 6.6 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Massive, Granular
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins
- Typical price
- $50-300 per specimen depending on size and association
Where rockhounds find paxite
Classic worldwide localities
- Kutná Hora, Czech Republic
- Jáchymov, Czech Republic
- Sainte-Marie-aux-Mines, France
Field-hunting tip
Look in hydrothermal veins country — that is the host setting where paxite typically forms. If you start seeing koutekite, domeykite, arsenic in float, you are in the right ground. Field specimens usually show a massive, granular habit, so train your eye for that shape before scanning the outcrop.




